In: International Journal of Earth Sciences, 2014, vol. 103, no. 1, p. 61-82
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In: Swiss Journal of Geosciences, 2008, vol. 101, no. 3, p. 637-650
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In: Swiss Journal of Geosciences, 2007, vol. 100, no. 1, p. 125-135
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In: Swiss Journal of Geosciences, 2011, vol. 104, no. 1, p. 1-29
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In: Swiss Journal of Geosciences, 2008, vol. 101, no. 2, p. 431-452
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In: Transactions of the Royal Society of Edinburgh: Earth Sciences, 2000, vol. 91, no. 1-2, p. 221-233
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In: Journal of Petrology, 1998, vol. 39, no. 5, p. 1025-1037
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In: Bulletin of the Geological Society of America, 2013, vol. 125, no. 1-2, p. 89-108
Prior to their Alpine overprinting, most of the pre-Mesozoic basement areas in Alpine orogenic structures shared a complex evolution, starting with Neoproterozoic sediments that are thought to have received detrital input from both West and East Gondwanan cratonic sources. A subsequent Neoproterozoic–Cambrian active margin setting at the Gondwana margin was followed by a Cambrian–Ordovician...
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In: Ordovician of the World : 11th International Symposium on the Ordovician System, Alcalá de Henares, Spain, May 9-13, 2011, 2011, p. 75-82
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In: Comptes Rendus Geosciences, 2009, vol. 341, no. 2-3, p. 239-252
In the general discussion on the Variscan evolution of central Europe the pre-Mesozoic basement of the Alps is, in many cases, only included with hesitation. Relatively well-preserved from Alpine metamorphism, the Alpine External massifs can serve as an excellent example of evolution of the Variscan basement, including the earliest Gondwana-derived microcontinents with Cadomian relics. Testifying...
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